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首页> 外文期刊>Progress in Oceanography >Inverse reconstructions of ecosystem flows in investigating regime shifts: impact of the choice of objective function
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Inverse reconstructions of ecosystem flows in investigating regime shifts: impact of the choice of objective function

机译:调查制度转变中的生态系统流量逆向重建:目标函数选择的影响

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Inverse analysis is increasingly used in ecosystem modelling to objectively reconstruct a large number of unknown flows or interactions from a small number of observations. This type of analysis may be useful in relating observed regime shifts in ecosystem structure to underlying processes. Inversions of ecosystem flow networks currently use a constrained least-squares solution which at the same time minimizes the squared norm (the sum of squares) of the reconstructed flows. This minimum norm (MN) inversion is thought to be a parsimonious solution to the ecosystem flow inverse problem, but it may well not reflect how ecosystems are organised. It has been proposed instead that ecosystems evolve to maximize energy/mass flows or that they maximize the information content of the network weighted by ecosystem flows (ascendancy). We used simulated inverse experiments, where inverse analyses are applied to simulations of flow networks, to explore objective functions different than the MN generally used. We could not compute inverse solutions that maximize ascendancy because the objective function is unbounded. We could calculate inversions that maximize flows; however, these generally overestimated the simulated flows, even though the simulations were designed to maximize flows. It appears that the ecosystem flow inverse problem is too under-determined (too few data relative to the number of unknowns) to allow the use of these maximizing goal functions. We introduce a new minimization that simultaneously minimizes the squared flows and the squared differences between flows. This smoothing minimization makes the inverse flows as even as possible and it helps with some technical issues with MN inversions. The simulated inverse experiments indicated that this smoothed norm (SM) is the most robust in comparative analyses of contrasting ecosystem states, such as those that can be associated with regime shifts. Like the MN inversion, the SM inversion has no ecological basis. However, it is a conservative norm that is less likely to produce false differences between the dynamics of regimes.
机译:在生态系统建模中越来越多地使用逆分析来从少量观测结果客观地重建大量未知流或相互作用。这种类型的分析可能有助于将生态系统结构中观察到的制度转变与潜在过程联系起来。生态系统流量网络的反演目前使用约束最小二乘解,同时最小化了重建流量的平方范数(平方和)。该最小范数(MN)反转被认为是生态系统流量逆问题的简化解决方案,但它可能无法反映生态系统的组织方式。取而代之的是,建议生态系统发展以使能量/质量流量最大化,或使生态系统流量加权的网络信息含量最大化(优势)。我们使用模拟逆实验,其中将逆分析应用于流网模拟,以探索与通常使用的MN不同的目标函数。因为目标函数是无界的,所以我们无法计算最大化上升的逆解。我们可以计算出使流量最大化的反演。但是,即使模拟被设计为最大化流量,但这些方法通常高估了模拟流量。似乎生态系统逆流问题的确定性太低(相对于未知数的数据太少),无法使用这些最大化的目标函数。我们引入了一种新的最小化方法,该方法同时最小化了均方流量和均方差之间的平方。这种平滑最小化使逆流尽可能均匀,并且有助于解决MN反演的一些技术问题。模拟的逆向实验表明,在对比生态系统状态(例如可能与政权转移相关的状态)的比较分析中,此平滑范数(SM)最稳健。与MN反演一样,SM反演也没有生态基础。但是,这是一个保守的规范,不太可能在政权动态之间产生错误的差异。

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